肥城煤田地质构造特征及其对底板突水影响  

Study on Geological Tectonic Features in Feicheng Coalfield and Its Impact to Floor Water Inrush

作　　者：张国苓[1] 魏久传[1] 尹会永[1] 

机构地区：[1]山东科技大学地球信息科学与工程学院

出　　处：《山东科技大学学报（自然科学版）》2008年第1期14-18,38,共6页Journal of Shandong University of Science and Technology(Natural Science)

基　　金：山东省中青年科学家科研奖励基金项目(2004BS08004)

摘　　要：在系统搜集肥城矿区勘探、生产资料的基础上,分析了肥城煤田的地质构造形态特征和分布规律,褶皱和断层的关系。结合肥城各矿的突水实例,分析了各种地质构造与底板突水的关系,发现构造条件影响甚至控制了矿区的开采地质条件,构造预测对矿井安全高效的生产具有重要意义。Based on the data come from exploration and mining periods, the paper analyzes the geological tectonic features and their development and distribution rules in Feicheng Coalfield, and the relationship between folds and faults. Based on the real examples of water inrush in Feicheng Coalfield, the paper analyzes the relationship between water inrush and geological structures. Geological tectonic conditions not only influence but also control the mining geological conditions in the mining area. So the accurate forecast of structures is very important for the safe and efficient coal production of the Feicheng Coalfield.

关 键 词：肥城煤田 构造特征 突水机理 

分 类 号：TD163.1[矿业工程—矿山地质测量]